Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regionsHilgard, Eugene W. (Eugene Woldemar)
Science
Soils, their formation, properties, composition, and relations to climate and plant growth in the humid and arid regions
Hilgard, Eugene W. (Eugene Woldemar)
Soils
Intimately correlated with the humus-substances of the soil, as well
as with its temporary contents of the carbohydrates (cellulose, gums
and sugars) from which humus is formed, is the multitudinous flora of
micro-organisms always present and exercising important functions in
connection with the growth of the higher plants. Extended researches
by Adametz, Schloesing and Müntz, Miquel, Koch, Fraenkel, Winogradsky,
Frank and many others, have thrown light upon the immense numbers and
great variety of minute organisms, especially of the bacterial group,
present in soils, and upon their distribution and activities in the
same. It has been shown that their numbers are greatest near (although
usually not at) the surface, decreasing rapidly downward and generally
disappearing wholly at depths between seven and eight feet; the latter
depth varying of course according to the nature and porosity of the
soil, and both depth and numbers being greatest in summer.
_Numbers of Bacteria in Soils._—Adametz found in one gram of soil,
38,000 bacteria at the surface, 460,000 at ten inches depth; in a
loam soil at the surface 500,000, at ten inches 464,000 in each gram
of earth. Of mould and similar fungous germs there were only 40 to 50
in the same, 6 species being true molds, while four were ferments,
including the yeasts of wine and beer. Fraenkel found in virgin land
from near Potsdam, a sudden, marked decrease at depths of from three
to five feet; while in earth from inhabited places within the city of
Berlin, considerable numbers were still present at eight and even ten
feet, in some cases.
In the researches lately made by Hohl at the bacteriological station
at Liebefeld, near Bern, it was found that in cultivated soils the
number of bacteria greatly exceeds the figures given by Fraenkel.
He found a gram of moist soil to contain from three to fifteen
millions of bacteria. In the cultivated soil of Liebefeld he found
5,750,000, in meadow land 9,400,000, in a manure pile 44,500,000 per
cubic centimeter. These figures seem high for so small a quantity
of material, but taking the average size of a bacterium, a cubic
centimeter might readily contain six hundred millions. (Grandeau, Ann.
Sci. Agronomique, vol. 1, p. 461, 1905).
Mayo and Kinsley (Rep. Kansas Exp’t Station for 1902-3) have
made elaborate investigations of the numbers and kinds of
bacteria found in various soils in Kansas, in connection
with different crops. It is noteworthy that in most cases
their figures exceed considerably those given by European
observers, as they often reach high into the millions, in
one case to over fifty millions, per cubic centimeter.[56]
[56] The mode of statement in the paper is not always quite clear as
to the manner in which the averages given were calculated. It must be
remembered that these data refer to cubic centimeters of soil, or about
twice the amount (1 gram) used by European observers.
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